Geochronological, geochemical and mineralogical constraints of emplacement depth of TTG suite from the Sinassi Batholith in the Central African Fold Belt (CAFB) of northern Cameroon: Implications for tectonomagmatic evolution
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文摘

Sinassi Batholith is made up dominantly of TTG suite.

Geochemical data show calc-alkaline metaluminous I-type signature.

Average emplacement depths estimates is constrained at ca 16–18 km.

Successive emplacement ages are ca 670–686, 661–666 and 644 Ma.

Setting is consistent with a subduction-related magmatic arc of Andean-type.

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